One main feature of the tectono-paleogeographic evolution of the southern branch of the Paleo-Asian Ocean was that there developed residual marine basins in for
A stretch of the modern hypersaline coastal plain of the Gulf of Cambay was cho-sen to examine the distribution of the microbial mat-related structures (MRS) on
Soft-sediment deformation structures induced by seismic liquefaction and/or fluidization receive much attention in sedimentological,structural and palaeoseismic studies.The direct record of larger ear